Deception Island deceptively active

In Antarctica, the South Shetland archipelago is home to Deception Island, a volcanic-rounded island that is 15 km in diameter with a shield volcano. The volcano is mainly basalt-andesite and was one of the first parts of Antarctica to be discovered, probably around 1820 by UK and USA sealers. It has the longest history of human occupation than any other site in Antarctica is the island served as a whaling station from the first 30 years of the 20th century, as the site of a British Antarctic station, then Chilean and Argentine stations.

Deception Island deceptively active

In Antarctica, the South Shetland archipelago is home to Deception Island, a volcanic-rounded island that is 15 km in diameter with a shield volcano. The volcano is mainly basalt-andesite and was one of the first parts of Antarctica to be discovered, probably around 1820 by UK and USA sealers. It has the longest history of human occupation than any other site in Antarctica is the island served as a whaling station from the first 30 years of the 20th century, as the site of a British Antarctic station, then Chilean and Argentine stations.

The flooded caldera of Deception Island

On the island the large bay of Port Foster is at the centre of the flooded caldera, which covers most of the island at about 9 km in diameter. It has a narrow entrance called Neptune’s Bellows that is only 230 metres-wide, with Raven Rock in the middle of the inlet submerged under 2.5 metres of water, making entrance to the bay difficult. Across the island there is Mount Pond, 539 metres high, then an unnamed peak at 576 metres, while the caldera itself has a depth of less than 200 metres. The caldera was formed following the largest-known Antarctic eruption that expelled 30-60 cubic kilometres of magma. The age of the eruption is unknown however scientists believe that the eruption was caused somewhat by regional geological activity.

The rift zone

Deception Island is in the middle of the Bransfield Strait, 125 miles north of the Antarctic Peninsula. The strait is part of a mini-rift that is opening at the rate of 1 cm per year and is the last of a series of transform faults and min-rifts that succeed south of the tectonic plate Scotia and joins in the far east the junction point between the African, South American and Antarctic plates. According to geologists the rift will be short-lived in geologically terms with some estimates that it will stop in a few hundred thousand years.

Monitoring volcanic activity

Humans have been recording volcanic eruptions on the island with the first in 1790, followed by eruptions in 1828, 1842. In the 20th century there were two volcanic eruption periods, from 1906 to 1910 and from 1967 to 1970. It was during the eruptions over 1967-1970 that the British and Chilean Antarctic stations were destroyed. Today the stations that are situated there is the original Argentine station and since the late 1980s Spain’s summer-only station.

Deception Island deceptively active

During the 1967 eruption, there was unrest in April followed by the new eruption on December 4th. The new eruption opened new vents along a 5-kilometre-long fissure in the northern part of the caldera and a new island formed on the western-side of what is known as Telefon Bay. In 1969, there was a short-lived eruption on the island with a series of fissures forming under a thin glacier about 100 metres thick over a distance of 4 kilometres. The eruption created a large and sudden discharge of meltwater that overflowed the glacier, severely damaging buildings on the island. Following this the volcano erupted again in 1970. The first signs that the volcano was about to erupt came from observers on research stations on the Antarctic Peninsula. O’Higgins Antarctic base (Argentina), located 170 kilometres from Deception Island, recorded a significant earthquake on August 12th. On August 13th, Bellingshausen Station, located 110 kilometres to the south, received an ash fall as well as a strong odour of sulphur. Meanwhile, other Antarctic stations along the Peninsula recorded similar events including electric storms. The eruption was one of the most violent even recorded on Deception Island with it beginning with phreatomagmatic explosions that are caused by the mixing of sea water and magma. The eruption opened fissures with 5 marine and 7 subaerial vents, one of which formed under glacial ice. The last main volcanic events on the island occurred in 1987 and 1991: In 1987 satellite images showed a plume from Deception Island on July 23rd that extended around 100 kilometres southeast. During this event, local seismic activity was detected but there was no evidence of an eruption found during later field surveys. Meanwhile in 1991 increased seismic activity and water temperatures were detected in the caldera during the summer sea by Spanish and Argentine scientists, however, no eruption occurred.

The volcano springs to life

Since 1989, the Spanish Antarctic Program has conducted monitoring at Deception Island during the summer period. This work is carried out by researchers from the University of Granada and University of Cadiz, Spain in collaboration with other research institutions. Over the period 2014-2015 the survey noted sustained deformation and increased seismicity. To gather data researchers, deploy a temporary seismic network made up of five three-component, short-period seismic stations and a small-aperture seismic array. Data from this network is transmitted to the Gabriel de Castilla Spanish base where it is analysed in real-time. Variations in distance between GPS stations since 2013 have revealed a steady increase in distance of around 5 cm/year. The 2014-2015 survey shows an accumulated deformation of 10 cm. The scientists believe this deformation is in response to a pressure source under Port Foster. Compared to previous years this seismic activity was considered to be intense with the total number of events recorded an order of magnitude larger than previous years and by far the most activity recorded since unrest in 1999. During this period both tectonic and volcano-tectonic-related earthquakes were common, but most were too small to be recorded adequately over the entire network so they could not be located. Nonetheless, the data recorded once cluster of earthquakes centred south-east of Livingston Island, which was active during the whole survey, and another cluster located south-west of Deception Island, with the remainder at distances of 5-20 kilometres.

A friendly alert system

Because the Spanish seismologists spend around three months each year on Deception Island (generally between Late November and late February), which also corresponds to the major period of human activity on the island, they also provide volcanic warnings to the island’s visitors including masters of vessels intending to arrive at the island and pilots of aircraft flying near the island. The warnings are colour-coded and come through bulletins from either Gabriel de Castilla Station (Spain) or from a spokesperson from one of the other national Antarctic programmes such as the Argentine Antarctic Institute, British Antarctic Survey or National Science Foundation. The alerts specifically are:

Green – no eruption is anticipated. During this time the volcano is quiet, in a dormant state, which is normal for the island

Yellow – no eruption is possible in the next few weeks and may occur with little or no warning. During this time the volcano is restless and there are increased levels of small earthquakes locally and/or increased volcanic gas emissions

Orange – explosive eruption occurring or is possible within a few days and may occur with little or no warning. During this time the volcano is erupting or about to erupt and there is an increased numbers and/or magnitudes of local earthquakes. When it does erupt ash plumes are not expected to reach 10,000 m above sea level. While around the volcano there may be lava flows visible

Red – major explosive eruption is in progress or will happen within a 24-hour period. During this time, large ash plumes are expected to exceed 10,000 m above sea level. Meanwhile, strong earthquakes are detected even at distant monitoring stations

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